[1]王小群,魏玉峰.西昌黄联土林的成因初探[J].水土保持研究,2007,14(01):218-220.
WANG Xiao-qun,WEI YU-feng.The Preliminary Analysis on Formation Mechanism of the Earth Forest of Xichang-Huanglian[J].Research of Soil and Water Conservation,2007,14(01):218-220.
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WANG Xiao-qun,WEI YU-feng.The Preliminary Analysis on Formation Mechanism of the Earth Forest of Xichang-Huanglian[J].Research of Soil and Water Conservation,2007,14(01):218-220.
西昌黄联土林的成因初探
《水土保持研究》[ISSN:1005-3409/CN:61-1272/P]
卷:
14
期数:
2007年01期
页码:
218-220
栏目:
出版日期:
1900-01-01
- Title:
- The Preliminary Analysis on Formation Mechanism of the Earth Forest of Xichang-Huanglian
- 分类号:
- P588.11
- 摘要:
- 西昌黄联土林位于安宁河左岸的谷坡地带，它是发育在一套冰水冻融泥石流堆积体之上的地貌景观。文中重点阐述了土林发育的自然地质背景：气候、地质构造、地形地貌、地层岩性、水文地质条件等，提出了土林是在特定的物质条件、地形地貌条件、内外动力地质条件、气候环境条件下形成的一种特殊地貌景观。具有一定规模的黄联土林拥有独特的观赏价值和一定的科学价值。
- Abstract:
- The earth forest of Xichang-Huanglian is located on the slope of the Anning River. It is a kind of morphology physiognomy which has developed into the debris flow deposits. The nature geological conditions-climate, geologic-conformation, morphology physiognomy and stratum lithology are expounded. The causes of form about the earth forest of Xichang-Huanglian are beacause of specifical substance, morphology physiognomy, inner-dynamic geologic process, outer-dynamic geologic process and climate environment. The particular view and admire and definite science worthiness of the earth forest of Xichang-Huanglian were described.
参考文献/References:
[1] 王兰生,王小群,等.四川省地质遗迹景观调查攀西分区报告[R].成都理工大学,2005.
[2] 明庆忠,刘丽娜,李春茂,等.丹霞地貌、土林地貌与旅游开发[J].云南师范大学学报,2005,20(3):63-67.
[3] 陈述云,张建云.元谋土林的形成条件及发育速率[J].云南地质,1994,13(4):383-390.
备注/Memo
收稿日期:2006-2-4;改回日期:。
基金项目:中国科学院知识创新项目“岷江上游生态极度退化区山地灾害综合防治试验示范”；攀枝花市-中国科学院科技成果孵化资金资助项目“攀枝花市灾害成因、规律性及对策研究”
作者简介:王小群（1972- ），女，副教授，博士研究生，主要从事地质工程、岩土工程、地质环境等研究。
更新日期/Last Update:
1900-01-01